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Record W4380589223 · doi:10.4271/2023-01-1458

3D Immersed Boundary Methods for the Calculations of Droplet Trajectories towards Icing Application

2023· article· en· W4380589223 on OpenAlexaff
Pablo Elices Paz, Emmanuel Radenac, Stéphanie Péron, Ghislain Blanchard, Éric Laurendeau, Philippe Villedieu

Bibliographic record

VenueSAE technical papers on CD-ROM/SAE technical paper series · 2023
Typearticle
Languageen
FieldEngineering
TopicIcing and De-icing Technologies
Canadian institutionsPolytechnique Montréal
Fundersnot available
KeywordsAerodynamicsImmersed boundary methodBoundary value problemBoundary (topology)SolverComputer scienceAirflowComputational fluid dynamicsTrajectoryFinite volume methodMechanicsMechanical engineeringMathematicsPhysicsMathematical analysisEngineering

Abstract

fetched live from OpenAlex

<div class="section abstract"><div class="htmlview paragraph">The in-flight ice accretion simulations are typically performed using a quasi-steady formulation through a multi-step approach. As the ice grows, the geometry changes, and an adaptation of the fluid volume mesh used by the airflow and droplet-trajectory solver is required. Re-meshing or mesh deformation are generally employed to do that. The geometries formed are often complex ice shapes increasing the difficulty of the re-meshing process, especially in three-dimensional simulations. Consequently, difficulties are encountered when trying to automate the process. Contrary to the usual body-fitted mesh approach, the use of immersed boundary methods (IBMs) allows solving, or greatly reducing, this problem by removing the mesh update, facilitating the global automation of the simulation. In the following paper, an approach to perform the airflow and droplet trajectory calculations for three-dimensional simulations is presented. This framework utilizes only immersed boundary methods. In particular, two methods are presented. On the one hand, a ghost-cell Immersed Boundary approach has been developed to solve the aerodynamics. The Euler equations are solved at fluid points, whereas the solution is forced in the vicinity of the obstacle at some particular cells (IB target points), in order to mimic a slip boundary condition. Special attention has been given to the applied boundary conditions as well as to the location of these IB target points. In fact, instead of the most commonly used approaches where the IB target points are placed in the solid or in the fluid, the case where these IB target points lie astride the obstacle (namely “GC Surrounding” in the following), in the fluid and solid regions, is studied. On the other hand, to solve the droplet trajectory equations, the penalization method, already present in IGLOO2D (the 2D ice accretion suite developed at ONERA), has been expanded to the three-dimensional simulations. The two immersed boundary methods are compared and numerically tested on different cases. First, a mesh refinement study is performed for weakly compressible flow around a cylinder. In this case, the solution is compared with that obtained using a body-fitted simulation and it serves as a verification of the method. Next, the approach is used in two other different cases. The first case involves an iced GLC305 airfoil, which is characterized by its complex geometry, under compressible subsonic conditions. The second case is a three-dimensional simulation in which the presented approach is used to analyze the weakly compressible flow around a sphere.</div></div>

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.001
metaresearch head score (Gemma)0.001
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Bench or experimental · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.881
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.001
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0000.002
Science and technology studies0.0010.001
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0010.001
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.022
GPT teacher head0.309
Teacher spread0.288 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

Study designBench or experimental
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations2
Published2023
Admission routes1
Has abstractyes

Explore more

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